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egoroff_w [7]
2 years ago
6

Consider the picture of the carbon cycle. Carbon dioxide is a small portion of the gases in our atmosphere. Carbon dioxide is na

turally added when organisms respire. It is removed naturally when plants and other producers undergo photosynthesis. State and explain the two different ways that humans are adding carbon dioxide to the atmosphere. Use the diagram below to help you; include words from the diagram in your answer.

Biology
1 answer:
aev [14]2 years ago
6 0

Answer:

Humans add to the carbon cycle by burning fossil fuels to make things run like factories and or running cars. People also add to the carbon cycle by resperating just like animals and when we die we get decompsed and add to it that way also

Explanation:

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Give one big reason why viruses are not alive
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because we killed them and follow the virus-safe rule..?

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household bleach has ph between 12 and 13. From. this information, which of the following best describes the bleach solution
andrew-mc [135]

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It would be a BASIC substance

Explanation:

Basic is the opposite of acidic

4 0
3 years ago
The half-life of carbon-14 is 5730 years. Radiocarbon dating can not be used to estimate the age of objects up to about 50,000 o
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False

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8 0
3 years ago
What determines the type of igneous rock that forms from magma? a. The heat and pressure the magma is exposed to b. Whether the
OLEGan [10]

Answer:

c. Magma composition and cooling rate.

Explanation:

A rock cycle can be defined as a concept used to describe the continuous process that leads to a rock's creation, formation, transformation from one form to another, destruction and reformation over a specific period of time. The natural phenomenons that influences the rock cycle are weathering, plate tectonic activity, erosion, etc.

Basically, the three (3) main types of rocks are; metamorphic rock, sedimentary rock and igneous rock.

All igneous rocks are produced from magma (lava) and formed at the Earth’s surface, thereby, causing them to have a coarse texture and dark colors.

Generally, the cooling and solidification of magma (lava) leads to the formation of an igneous rock, either when the melted rock is still inside the continental crust of the Earth or at volcanoes on the Earth's surface.

Hence, magma composition and cooling rate determines the type of igneous rock that forms from magma. Some examples of an igneous rock are granite, obsidian, tuff, basalt, rhyolite, andesite, pegmatite, dacite, scoria, pumice, etc.

4 0
2 years ago
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